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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Table 2. Comparison of Flood Frequency - Blue River below Dillon Dam <br />Method of Analysis 10-yr 50-yr 100-yr <br />Inflow 2730 3660 4070 <br />(USGS Regression Equations) <br />FIS outflow <br />LP3 outflow (Computed value) <br />0.05 Confidence limit <br />0.95 Confidence limit <br />Ratio of inflow to outflow <br />FrS <br />LP3 <br /> <br />500-yr <br />4940 <br /> <br />2500 <br />1960 <br />1670 <br />2410 <br /> <br />3100 <br />2770 <br />2270 <br />3660 <br /> <br />3350 <br />3130 <br />2520 <br />4240 <br /> <br />3800 <br />3980 <br />3100 <br />5700 <br /> <br />91.6% <br />71.8% <br /> <br />84.7% <br />75.6% <br /> <br />82.3% <br />76.9% <br /> <br />76.9% <br />80.6% <br /> <br />It appears that the FIS hydrology for reservoir outflow assumed a decreasing routing <br />factor for Dillon Reservoir. The available data shows that this is probably not a good <br />assumption since the reservoir volume is relatively fixed so that larger inflows will have <br />less attenuation. The LP3 estimate of outflow follows the pattern of increasing routing <br />factor that is more consistent with reservoir operations. <br /> <br />Our understanding of Dillon reservoir operations is that Denver Water draws down <br />the reservoir during the month of May, based on snow pack information. The amount of <br />control they can provide is relatively fixed and depends on the volume of water that can <br />be released in May through the outlet works. As indicated by the LP3 analysis, it is <br />likely that large floods (greater than 100-year) would not be reduced as much as the <br />original FrS analysis indicated. <br /> <br />The difference between the LP3 values and the 1978 FIS values is small. The FrS <br />estimate of the 1O-year flood is the only value outside of the confidence limits with a <br />value that is 540 cfs (about 28-percent) higher than the flow computed from the LP3 <br />analysis. The 50- and 1 O-year floods are probably slightly lower than the FrS originally <br />estimated but, because of dam operations, the LP3 analysis is not reliable. The past <br />record of operation indicates that Denver Water cart effectively control a 10-year flood <br />and may be effective up to nearly the 50-year flow. <br /> <br />We recommend that the previous FrS hydrology be used for the updated FIS since the <br />two are not significantly different. It is understood, however, that this hydrology appears <br />to be somewhat inconsistent with the operation of Dillon Dam. Current operations by <br />Denver Water probably reduce flood magnitude in the Blue River below what the FIS <br />estimated in 1978 for the 10- and 50-year floods and would not be as effective for <br />controlling the 500-year flood. <br />